How well do we understand the dynamics of stratospheric warmings?
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The changing magnitude of the vorticity gradients between zonal velocity maxima and minima gives rise to a staircase pattern of absolute vorticity and potential vorticity as a function of latitude.
“The changing magnitude of the vorticity gradients between zonal velocity maxima and minima gives rise to a staircase pattern of absolute vorticity and potential vorticity as a function of latitude (McIntyre 1982;Dritschel and McIntyre 2008).”
From Mechanisms of Jet Formation on the Giant Planets (2010) · cites this paper as McIntyre 1982
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- Authors
- McIntyre, M. E.
- Affiliations
- Department of Applied Mathematics and Theoretical Physics
- Corresponding author
- McIntyre, Michael E.
- ORCID
- McIntyre, Michael E.
- Venue
- Journal of the Meteorological Society of Japan Ser II
- Published
- 1982
- Volume
- 60
- Issue
- 1
- Pages
- 37-65
- ISSN
- 0026-1165 (ISSN-L)
- 2186-9057
- OpenAlex
- W2523027480
- Cited by
- 317
- References
- 98
- Citations by year
- 2026: 5 · 2025: 10 · 2024: 6 · 2023: 3 · 2022: 16 · 2021: 18 · 2020: 11 · 2019: 13 · 2018: 12 · 2017: 11 · 2016: 10 · 2015: 6 · 2014: 10 · 2013: 6 · 2012: 11
- FWCI
- 11.88
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Journal of the Meteorological Society of Japan Ser II (publishedVersion)
- Funders
- Met Office
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Atmospheric Ozone and Climate
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Meteorological Phenomena and Simulations
- Keywords
- sudden stratospheric warming, stratospheric dynamics, stratosphere-troposphere coupling, spurious resonances
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